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lding yge the subarctic Precambrian Shield region. As measured in water samples collected over a 12 year period (1997–2008), the levels of evaporative isotopic enrichment in both lake and watershed outflow were dif-mon f or intermittent runoff. This variability is driven by fluctuations in storage,...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.587.4704 http://www.science.uwaterloo.ca/~jjgibson/mypdfs/bakercreek.pdf |